Validation of lidar temperature measurements in the stratosphere over Tomsk on aerological and satellite data for 2015-16 years
Vestnik KRAUNC. Fiziko-matematičeskie nauki, no. 4 (2017), pp. 57-63 Cet article a éte moissonné depuis la source Math-Net.Ru

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The vertical temperature distribution in the lower stratosphere is compared with the data of lidar, radiosonde, and satellite measurements. In the lidar measurements, Raman and Rayleigh channels for receiving scattered light at wavelengths of 607 nm and 532 nm were used. Taking into account the spatio-temporal separation of the measurements, a qualitative and quantitative correspondence of the vertical temperature profiles was obtained. The prospects of using the Raman scattering method for measuring temperature in the lower stratosphere are shown.
Keywords: temperature, stratosphere, Raman and Rayleigh scattering of light, radar
Mots-clés : radiosonde, «Aura»satellite.
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V. N. Marichev; D. A. Bochkovsky. Validation of lidar temperature measurements in the stratosphere over Tomsk on aerological and satellite data for 2015-16 years. Vestnik KRAUNC. Fiziko-matematičeskie nauki, no. 4 (2017), pp. 57-63. http://geodesic.mathdoc.fr/item/VKAM_2017_4_a5/

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